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Reservoir sedimentology of the M. Triassic Halfway Fm. , Wembley field, Alberta

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (United States)
OSTI ID:7079428
 [1]
  1. Univ. of Alberta, Edmonton (Canada)
The Middle Triassic Halfway Formation of west-central Alberta is interpreted as a prograding barrier island shoreline deposit. A detailed sedimentological study based on 130 cored sequences and 300 well logs in the Wembley area (Townships 72-73, Ranges 7-9, West of Sixth Meridian) has enabled the author to delineate the geometry of reservoir units, interpreted as tidal inlet fill, upper shoreface, and flood-tidal delta sandstones. Complete shoreface sequences average 15 m in thickness and form mappable trends tens of kilometers along depositional strike, but are only continuous for a few kilometers across dip, with the intervening areas having been reworked by one or more migrating tidal inlets. The strike-elongate inlet-fill sequences cover more than 50% of the field area. They are typically 10 m thick and exhibit the best porosities due to leaching of bioclastic material in the lower part of the fill, but the down-cutting of successive inlets makes the reservoir sands laterally discontinuous. Inlet sands extend up-dip into flood-tidal delta sandbodies that average 4 m in thickness and pinch out in lagoonal muds. Although showing much greater lateral continuity than the other reservoir units, the upper shoreface sandstones do not exhibit biomoldic porosity and are a less productive unit. Such an understanding of the architecture of the various reservoir components present in a barrier island shoreline system is essential when planning a secondary recovery program.
OSTI ID:
7079428
Report Number(s):
CONF-910403--
Conference Information:
Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (United States) Journal Volume: 75:3
Country of Publication:
United States
Language:
English

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